Soils are formed by a series of processes commonly referred to as

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Soils are formed by weathering, which involves the breakdown of rocks, minerals, and organic matter in the Earth's crust. This process is typically driven by physical, chemical, and biological agents. Weathering gives rise to soil particles that accumulate and become mixed with various organic and inorganic materials to form the different layers and horizons that make up a soil profile. While sedimentation and diagenesis can contribute to the formation of sedimentary rocks, they are not directly involved in the formation of soils. Similarly, lithification refers to the processes by which sediments are compacted and cemented to form rocks, and is not directly relevant to soil formation.

Soils Are Formed by a Series of Processes Commonly Referred